The age of three terminal glacial deposits located at Hoås, Gikling and Romfo in the Sunndalen valley, Møre & Romsdal, has been uncertain. The aim of this study has been to document these deposits to clarify the chronology ...

The thickness and extent of the inland ice during the Younger Dryas Chronozone (YD) in central parts of South-Norway is still debated. The aim of this thesis is to map the sediments in Grødalen, for reconstruction of the ...

We present a new time-slice reconstruction of the Eurasian ice sheets (British–Irish, Svalbard–Barents–Kara Seas and Scandinavian) documenting the spatial evolution of these interconnected ice sheets every 1000 years from ...

This study is part of a broader palynological investigation of late Middle to Late Triassic, where the main aim is to improve the biostratigraphic resolution by applying palynology. The low abundance of macrofossils (e.g. ...

This study presents palynostratigraphic and
palynofacies analyses from the shallow
stratigraphic core 7830/3-U-1, drilled through
the Snadd Formation (equivalent to De Geerdalen
Formation) offshore Kong Karls Land in ...

Two well dated lateglacial relative sea-level curves have been constructed from
Hordaland, western Norway, by the isolation basin method. The easternmost curve is
based on six basins from the Os area, close to the Younger ...

An updated Late Neogene dinoflagellate cyst biozonation of the Norwegian Sea is needed, as it, together with other recent zonations from the Iceland Sea, the eastern North Atlantic and the eastern North Sea (Denmark), will ...

This study presents a structural analysis, from macro- to micro-scale, of the Permian carbonates and spiculites of the Kapp Starostin Formation. The analysis was conducted to better understand the fracture development and ...

The origin of the mountainous topography in southern Norway is at present unresolved. Post-Devonian sediments are absent onshore, making quantification of crustal uplift and fault displacements difficult. Low-temperature ...

The development of the Caledonian orogen to a passive margin leaded to the present-day Norwegian landscape. The most recent denudation history in Mesozoic and Cenozoic times holds the key to the morphotectonic development ...